The radiative and geometric properties of melting first-year landfast sea ice in the Arctic
Nathan J. M. Laxague,Christopher J. Zappa,Andrew R. Mahoney,John Goodwin,Cyrus Harris,Robert E. Schaeffer,Roswell Schaeffer Sr.,Sarah Betcher,Donna D. W. Hauser,Carson R. Witte,Jessica M. Lindsay,Ajit Subramaniam,Kate E. Turner,and Alex Whiting
National Institute of Water and Atmospheric Research, Te Whanganui ā Tara / Wellington, Aotearoa / New Zealand
Alex Whiting
Native Village of Kotzebue, Kotzebue, AK, USA
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Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 1,316 (including HTML, PDF, and XML)
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Total article views: 1,118 (including HTML, PDF, and XML)
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Total article views: 198 (including HTML, PDF, and XML)
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The state of sea ice strongly affects its absorption of solar energy. In May 2019, we flew uncrewed aerial vehicles (UAVs) equipped with sensors designed to quantify the sunlight that is reflected by sea ice at each wavelength over the sea ice of Kotzebue Sound, Alaska. We found that snow patches get darker (up to ~ 20 %) as they get smaller, while bare patches get darker (up to ~ 20 %) as they get larger. We believe that this difference is due to melting around the edges of small features.
The state of sea ice strongly affects its absorption of solar energy. In May 2019, we flew...